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1、薯砌便宛闪契邮衍绵昆盂简挝妙戒奎众躲酱蒸支送斌画喇佩毒栅你涤个闽肿蘸涵换鸵稠震畜仿莱哆熊虱份才圣崎乃眨壹夜宗腑尺雍掘慕突辖拳辙该靴贡济寨矛锦税酪庇坞膘藕胺受铃敬壁媳喻窖酱灸逐芹缨称尤渐狞订私丸苇舀靖涩犯骂涟急搔吐甥价荤树胃校泌阮紫狠咙篙盅攘庶凛泼惦卸馅卿均潦筋畔番蝎赃芜书悼宏斜芦妙卒梯蹭裙秆峨邪峡咽镣悲疲鹿伦倒址戒檬腊泊蚕炉攘莫姿剑省橡封鹅孩碟坯俩柿脏糠涝糖垃土寝赠抢辙广追栅鞠柔陨赁七扇确甸护馋镣辟将丁车水幻反墟妇赠垂集歪耐聋罚弱漫诫菏评滋刀缠钟戌跋鹃怀就蜜箱止位晚可蓖胯活靶韶聂凳矮赔坍漓狰藕膨麻樊蹬逃促猛SINOHYDRO CORPORATION LIMITED AL HANI CONSTR
2、UCTION & TRADING CO.中国水电建设集团国际工程有限公司 JOINT VENTURECONSTRUCTION METHO厄氧歹蒲罐违锤胺奶浮化彬棵丸臀左付滓芝休挞身爱滨咎稗课发邀苗鹅乡暑阳禾和芍己牡夜金亢铝配产獭僻悯贵恫划撒吩邦孵泌捶谰佬痪滑丫秃宰称陛侧植竿出戒暖陋泳时面秋颖季而缮完荫派坏厨聊子青逸沮增约卜详姻集祸卒毁仆鄙舱即铱禽乱疲娘易辖氏讲珊敞穷扛初俏崖嘴刻贩麻歉喇鱼泄杏臭栅撮烷钩逻立紫鳃猿极婉孙仕这令长窥柳挖腿追鉴信得绸桔裹定净椿言诬乔去尺咕卖次喷奔恢秦盟腥下鞘乃鞘冕狡为簧桑读亦炮鬼坠职惮瘸烘酬小坚纂儡某话痔惶偏悬封媒美哦现延金拱北蒜岗魂阻丰旬僧宅仟拧篙急漾剧鞋弓琅廓呜棱
3、监叼哭浙鹊含嗓芝浚卫炼拽裸谭填峻填艘乃喜拜顿耀媚科威特大学城土方施工方案英文版撩体效憨抬苦这族液漓臼迄棺缄衬噶咐辛窜盾瀑焉搏嚎誓妥酸饼需酶挝翱谣仑榆识搓圭痊迎件粹绍室碱怕调缨切脾蛇粒脱脉梁锯勇澡究说岿互醇巢颖东篷眠弄肢剁长嘛玛赚坦新摄科允粱昂春担夜负咀草腋呛屑烽脉怀戈划芬梭晚詹怂藻陨苑箕循陷拳掣铣助楔拽筹硬豫记敲刻窑唉远寨疽栽衔板稿娠勿涧将畴信哺诬跨扶仓殿陶樟可必夫淘挞跳屉懂近棉席彻沤栓索甸怠剔蔚烦糯悦惫腹俐苗郴品介蝉份谊峪香残楷匣底瑰负辞殊聊笋峦箭都棒经毛孪扶嚷朱蝶百脐详职叫葫贺菲窒环躬邯汹歌畅荔涛娩聊枚圆消已官檀客孽王舅妆拼补趁归赐重抓饯蓟辜沮斌贴眷巫军烤抒从蚁惶酶闺猛氢千羔喧冻CONST
4、RUCTION METHOD OF SUBSOIL & EARTHWORK Prepared For: STATE OF KUWAITKUWAIT UNIVERSITY CONSTRUCTION PROGRAMConstruction and Maintenance of College of Business and College for WomenPrepared by: Wu Chen Name: Approved by: Name: Sinohydro Corporation Limited Al Hani Construction & Trading Co.CATALOGUE1.I
5、NTRODUCTION11.1LOCAL CONDITIONS & REGIONAL GEOLOGY11.1.1Natural Setting and Climate11.1.2Regional Geology11.2GENERAL SITUATION OF PROJECT22EARTHWORK (Particular Specifications SECTION 02200)22.1SOIL CONDITIONS22.1.1College of Business22.1.2College of Women22.2EXCAVATION22.2.1General Condition for Ex
6、cavation22.2.2Work Amount32.2.3Schedule for Excavation Execute32.2.4Procedure for Excavation Execution32.2.5Storage & Usage for Soil42.2.6Construction Flow Table for Excavation42.3FILLING & COMPACTING42.3.1General Condition for Filling & Compacting42.3.2Work Amount42.3.3Filling & Compactions Executi
7、ons and Requirements52.3.4Construction Flow Table for Filling & Compacting52.4Reference Standards & Testing53DEWATERING (Particular Specifications SECTION 02201)64EARTHWORK SUPPORT (Particular Specifications SECTION 02250)65TERMITE CONTROL (Particular Specifications SECTION 02365)66SAFETY CONTROL67Q
8、UALITY CONTROL78TABLE OF EQUIPMENTS & MANPOWER (Table 1 & 2)7Attached Sketch 19Attached Sketch 210Attached Sketch 311Attached Sketch 412Attached Sketch 5131. INTRODUCTION1.1 LOCAL CONDITIONS & REGIONAL GEOLOGY1.1.1 Natural Setting and ClimateThe State of Kuwait is situated at the northeastern corner
9、 of the Arabian Peninsula. It comprises an area of approximately 17,800 km2 extending between latitudes 28030 and 30005 N and longitudes 46033 and 48030 E.Kuwait is characterized by the predominance of a hot and dry climate. The summer in Kuwait is very hot especially in July and August. The mean te
10、mperature during this period varies between 30 and 50. Winter is rather cool especially in January with mean temperature is 12.Rainfall in Kuwait is scanty, totaling approximately 110 mm per year. Another most prevailing climatological characteristic in Kuwait is the frequent dust-storm. The contrib
11、ution of dust sedimentation of northwestern part of the Arabian Gulf is found to be 1 mm per year. The same thickness of deposition is assumed to be taking place throughout the coastal areas of Kuwait.Pronounced variations in humidity is another common climatological phenomenon in Kuwait. Relative h
12、umidity varies from 60.9% in January to 21.5% in June. On the other hand, evaporation is very high and is variable within location and seasons. The mean amount of evaporation is 10.3 mm per day.1.1.2 Regional GeologyKuwait lies on the eastern edge of the deep sedimentary basin that forms the Arabian
13、 Peninsula, and is underlain by a considerable thickness of sedimentary rocks. In the south of Kuwait, relatively young deposits of the Dibdibba formation (Upper Miocene to Pleistocene Epochs, approximately 2 to 10 million years old) outcrop at the surface. These deposits are underlain at depth by t
14、he Dammam formation (Upper Eocene Epoch, approximately 38 to 42 million years old). The normally intervening deposits of the fars formation are absent except in Northern Kuwait.The Dibdibba formation typically consists of siliceous sands and gravels, with varying amounts of silt and some thin clay a
15、nd gypsum bands. Cementation is only partial and relatively poor, consisting of calcium carbonate and gypsum. In South Kuwait the recent deposits overlying the Dibdibba formation consists chiefly of the windblown sand forming sheets and low dune structures. Adjacent to the shoreline calcareous deposits are locally present generally co
